肱骨骨干骨密质厚度的二维可视化及其定量分析

形态示量图是一种展示三维形态测量信息的二维可视化手段,能有效地反应骨密质厚度的分布特点。虽然现代人、更新世古老型人类和大猿的骨密质厚度分布存在差别,但全新世现代人内部是否有变异存在尚未被充分研究。本文选择全新世华中、华北地区的6个农业人群的34例右侧肱骨标本（23例男性、11例女性）,使用形态示量图对其骨干骨密质厚度的分布特征进行了全面分析。在方法上,本文比较了通过厚度最大值和生物力学长度对骨密质厚度进行标准化后分析结果的差别,并验证了主成分分析在形态示量图上的适用性。结果显示,在全新世华中、华北地区的农业人群中,男、女的厚度分布模式存在一定差异,而不同人群男性的差别并不明显。本文虽通过全新世华中、华北地区的农业人群揭示出全新世现代人在肱骨骨干骨密质厚度分布上存在一定程度的变异,但仍需在未来工作中依托本文方法,选择人群种类更丰富、标本量更大、个体变量控制更严格的材料,进一步验证或扩展本文所得结论。     

辽宁建平古人类肱骨形态结构分析

1957年,在辽宁省建平县发现了一根古人类肱骨化石,编号PA103。通过同一批龙骨中筛选的哺乳动物化石,吴汝康推断PA103应该为更新世晚期古人类,并对该化石进行了表面形态特征观察和描述。为了对PA103化石的内外结构进行更全面的了解,除了线性测量数据的对比,本文还通过计算机断层扫描技术,结合生物力学和形态示量图分析对建平古人类右侧肱骨化石PA103进行了分析。通过本研究发现,PA103骨干横断面的生物力学粗壮度和力学形状指数明显小于尼安德特人,而与同时期欧亚大陆古人类不利手侧最为接近,这说明建平人右侧肱骨可能不是惯用手,同时,建平人的行为活动应该与同时期同地区的古人类处于同一水平,而小于尼安德特人。整体来看,PA103骨干骨密质厚度和截面惯性矩与近现代人的分布模式较为接近,除局部数值增大外,其整体数值小于近现代人的平均水平,这可能与遗传或行为活动有关,由于缺少古人类化石对比数据,更详细的了解还需后期开展更多相关的研究。     

山东新泰乌珠台人类牙齿的形态学特征

近些年在东亚发现的晚更新世现代人化石及其研究使得关于该地区现代人起源问题更加复杂,更多该时段人类标本的研究有助于对其有更清晰的认识。1966年在山东新泰乌珠台发现一枚古人类下颌臼齿,吴新智和宗冠福(1973)对其进行了报道,而后再无详细研究。本文将使用牙齿非测量性状的半定量化(分级)、齿冠外轮廓形状的几何形态测量、基于显微断层扫描(Micro-computed tomography 或micro-CT)的釉质厚度、釉质厚度分布规律和齿质表面三维结构复原等方法对乌珠台人类牙齿进行综合研究,进而对东亚晚更新世古人类牙齿形态特征变异有一个进一步的了解。结果显示,乌珠台人类牙齿的形态特征基本与现代人接近,但其所表现出的三角座横脊、Y型齿沟排列、原附尖在现代人中出现率较低,而更多发现在直立人或尼安德特人中。相对于东亚其他晚更新世现代人,乌珠台M3所表现出的特征组合具有特殊性,增加了东亚晚更新世现代人的牙齿形态特征多样性。未来研究可尝试测定乌珠台人类牙齿的绝对年代,以更好的将其归入到现代人演化序列中去。     

山西襄汾石沟砂场发现人类枕骨化石

2012年,山西襄汾县南贾镇上鲁村石沟砂场发现一件人类枕骨化石。该化石埋藏于汾河西岸第Ⅲ级阶地的砂砾层,地质时代可能是中更新世晚期。本文对枕骨形态特征进行描述,并将其与亚洲直立人、早期智人、早期现代人相关标本进行对比。观察发现,石沟古人类具有印加骨的形态特征,为中国古人类印加骨高频出现增添了新的证据;枕鳞中部没有发育枕骨圆枕,而具有最上项线,显示出枕骨形态的进步性,推测石沟古人类可能属于早期现代人。石沟古人类枕骨化石对于探讨中国及东亚地区古人类的系统演化问题提供了证据。     

东亚中更新世古人类下颔第二臼齿釉质-齿质连接面三维形状和釉质厚度分布

东亚中更新世古人类在头骨、下颌骨、牙齿等解剖部位表现出不同程度的形态多样性,中期成员代表为直立人,而晚期成员的演化地位具有较大争议。为进一步了解东亚中更新世古人类内部的形态变异特点和为东亚中更新世晚期古人类分类提供依据,本文使用微分同胚的表面匹配（Diffeomorphic Surface Matching, DSM）和形态测量图（Morphometric map）对下颌第二臼齿（M₂）釉质-齿质连接面的形状和齿冠侧面釉质厚度分布模式进行了量化分析。结果显示：1）东亚中更新世古人类与晚期人属成员（尼安德特人和现代人）存在较明显的形态差别;2）该时段晚期的东亚古人类相对中期直立人在侧面釉质厚度分布规律上具有独特性,并在釉质-齿质连接面的三维形状上与晚期人属成员更加接近。本文在以往对东亚中更新世古人类牙齿内外结构单个性状研究的基础上,使用三维形态测量方法进一步量化了M₂釉质-齿质连接面三维形状和侧面釉质厚度分布模式两项重要特征的变异特点,这对未来该时段同类型牙齿的形态鉴定以及解决东亚中更新世晚期古人类的分类地位具有一定意义。     

现代各主要人群中面部3D几何形态的对比

中面部的形态是个人识别的重要依据,并且长期以来都在各人种的形态对比研究中占有重要的地位。而中面部骨骼形态复杂,骨骼表面不规则,很难用传统的方法来进行测量和比较。本文采用基于三维表面半标志点的几何形态测量学研究东亚现代人中面部的形态及其变异范围,并与其他各大地理位置中的现代人群的中面部形态进行对比,为人类演化和对比不同人群的形态研究建立基础数据。本研究结果显示中面部形态能够大致区分各个现代人群,其中东亚现代人与除美洲印第安人以外的所有现代人的中面部形状之间都具有较为明显的差异。东亚现代人与澳大利亚和非洲的现代人中面部形状之间的差别最明显,而与欧洲和东南亚现代人的分布范围有部分重叠。东亚现代人群中面部的平均形状却具有非常明显的特点:沿着正中矢状面的结构回缩,而两侧的结构向前方和两侧突出。而其他现代人群的中面部平均形状则呈现出相反的特征,即沿着正中矢状面的结构为突出,而两侧的结构回缩的特征。这些特点在东亚发现的化石人类标本中也有很高的发生率,这表明这些中面部特征在东亚人类进化的序列是连续的,并无受到干扰的迹象。     

大荔颅骨在人类进化中的位置

本文将大荔颅骨的一系列形态特征与中国的直立人、欧洲和非洲的中更新世人、欧洲和亚洲的尼安德特人、中国和欧洲的早期现代人以及现生现代人的数据进行比较,发现可以归纳为几种状况。大荔颅骨:1)与其他中更新世颅骨比较一致,而与早期现代人相去较远;2)与早期和现生现代人一致或接近,显得比其他中更新世人进步;3)在中国早期现代人或现代人变异范围内,也在欧洲中更新世人变异范围内或与之接近,却与中国直立人相距较远;4)处于一般中更新世人与早期现代人之间的中间状态;5)处于中国直立人与中国早期现代人之间的中间位置,而且比较接近欧洲/非洲中更新世人;6)与东亚多数化石人比较一致,而与旧大陆西部中更新世化石人相去较远;7)与中国直立人显然不同,而与欧洲/非洲中更新世人更加接近;8)与非洲中更新世人接近,而与中国直立人和欧洲中更新世人差距较大;9)与大多数中更新世人不同,似乎是自身独有或罕见的。基于这样复杂的状况,作者提出,大荔颅骨既不属于直立人,也不属于海德堡人,表现为兼具东亚的直立人、欧洲和非洲中更新世人的特征,而且是这些共有特征与早期现代人部分特征的镶嵌体,可能比中国的直立人对中国现代人的形成做出过更大的贡献。     

降钙素对骨质疏松大鼠骨密度形态计量学与骨代谢的影响

目的探讨降钙素(密盖息)对骨质疏松大鼠骨密度、骨形态计量学影响以及与血钙、磷、维生素D代谢和生长因子的关系。方法用摘除大鼠双侧卵巢的方式制备骨质疏松模型(OVX),实验动物分为4个组:模型对照组、密盖息治疗组,盐酸雷洛昔芬治疗组,假手术组。应用HOLOGIC第4代双能X线4500W骨密度仪测定大鼠腰椎、股骨上段骨密度值(BMD);以骨形态计量学测股骨骨小梁面积、矿化沉积率;用ELISA法测定血清IGF-1水平和血清25OHVitD浓度以及血淋巴细胞维生素D受体(VDR)含量。结果密盖息治疗组、盐酸雷洛昔芬治疗组均较OVX组腰椎、股骨上段骨密度增高,组间比较差异有显著性(P<0.01)。密盖息治疗组较盐酸雷洛昔芬治疗组股骨上段骨密度增高,两组之间差异有显著性(P<0.01)。密盖息治疗组骨小梁面积明显增加、矿化沉积率增高。密盖息治疗组、盐酸雷洛昔芬治疗组血清IGF-1浓度值、血清25-OHVitD浓度值升高,与OVX组比较差异有显著性(P<0.01)。各组血淋巴细胞VDR含量无明显变化,与OVX组比较差异无显著性(P>0.05)。结论密盖息能够预防腰椎、股骨上段骨密度丢失,使骨小梁面积明显增加、矿化沉积率增高并且血清IGF-1及血清25-OHVitD浓度值升高,但对VDR含量无明显作用。     

安徽东至华龙洞出土的人类化石

2006年在安徽省东至县华龙洞发现了1枚人类下颌第二臼齿和2件可以拼接在一起的额骨碎片化石。根据华龙洞动物群组成及地层情况,初步确定华龙洞化石层的时代为更新世中期。本文对在华龙洞发现的人类头骨和牙齿化石的形态特征进行了观测,并与相关古人类标本进行了对比。研究发现:华龙洞人额骨和下颌臼齿都呈现出一系列常见于东亚直立人的特征。华龙洞额骨曲度较小,具有粗壮的颞线和较厚的骨壁。此外,华龙洞额骨还具有额中缝结构和扩大的额窦。华龙洞下颌第二臼齿总体显得比较粗壮。齿冠咬合面具有第五尖、第六尖和第七尖。齿冠尺寸明显大于早期现代人、现代人类和欧洲更新世中期人类,位于直立人变异范围。结合对华龙洞人类额骨和牙齿形态对比所揭示的形态特点,在华龙洞发现的人类化石可能代表着生活在更新世中期的直立人。     

贵州毕节韦家洞古人类遗址年代测定及人牙的形态学意义

2007年贵州毕节韦家洞首次发现古人类活动遗物。2016~2018年对遗址做深入考察,发现韦家洞是一个严重破坏的晚更新世古人类遗址,在深度破坏的扰乱层中出土了大量古人类活动证据,包括石制品、动物烧骨和人类牙齿,2018年在洞口和洞内深处发现残留的原生文化层。本文报告了韦家洞原生文化层的¹⁴C年代测定结果,距今1.2~2.7万年前,属于晚更新世末期。同时,观察描述了韦家洞出土的一枚古人类上颌第四前臼齿化石,对牙齿形态测量进行了研究比较,发现韦家洞人牙测量值落在现代中国人变异范围内,牙冠咬合面及釉质-齿质交界面EDJ形态简单,牙根短,根管简单纤细,与现代人相似。牙冠颊舌径大,具有三角形隆起和齿带,牙冠颊侧和舌侧均有垂直沟,近中和远中缘有边缘副结节,牙根中部膨大,这些特征显示了韦家洞人牙形态的原始性。综合比较国内外出土的古人类上颌第四前臼齿的形态特点及其演化趋势,结合遗址年代测定结果,我们认为韦家洞出土的人类上颌第四前臼齿形态特点体现了古人类牙齿演化的镶嵌性,为晚更新世东亚早期现代人的形态变异及其演化增添了新证据。     

Fossil Homo femur from Berg Aukas,northern Namibia

The proximal half of a hominid femur was recovered from deep within a paleokarst feature at the Berg Aukas mine, northern Namibia. The femur is fully mineralized, but it is not possible to place it in geochrono logical context. It has a very large head, an exceptionally thick diaphyseal cortex, and a very low collodiaphyseal angle, which serve to differentiate it from Holocene homologues. The femur is not attributable to Australopithecus, Paranthropus, or early Homo (i.e., H. habilis sensu lato). Homo erectus femora have a relatively longer and AP flatter neck, and a shaft that exhibits less pilaster than the Berg Aukas specimen. Berg Aukas also differs from early modern femora in several features, including diaphyseal cortical thickness and the degree of subtrochanteric AP flattening. The massive diaphyseal cortex of Berg Aukas finds its closest similarity within archaic H. sapiens (e.g., Castel di Guido) and H. erectus (e.g., KNM-ER 736) samples. It has more cortical bone at midshaft than any other specimen, although relative cortical thickness and the asymmetry of its cross-sectional disposition at this level are comparable with those of other Pleistocene fem ora. The closest morphological comparisons with Berg Aukas are in archaic (i.e., Middle Pleistocene) H. sapiens and Neandertal samples. © 1995 Wiley-Liss, Inc.     

A note on the KNM-ER 999 hominid femur

The KNM-ER 999 hominid femur, in light of improved knowledge of later Pleistocene human postcranial morphology and ongoing reassessments of the emergence of modern humans in Africa, appears morphologically aligned with early modern humans rather than with late archaic humans. This is reflected especially in its having a clear pilaster, a proximally positioned minimum diaphyseal breadth (thereby lacking a proximo-medial diaphyseal buttress) and an exceptionally high neck-shaft angle. In these features, and especially the fast, it shows affinities to the Levantine Qafzeh-Skhul early modern human sample. However, the uncertainty regarding its stratigraphic provenience (early Late Pleistocene versus early Holocene) makes its relevance to the emergence of modern humans in Africa tenuous.     

A Hominin Femur with Archaic Affinities from the Late Pleistocene of Southwest China

The number of Late Pleistocene hominin species and the timing of their extinction are issues receiving renewed attention following genomic evidence for interbreeding between the ancestors of some living humans and archaic taxa. Yet, major gaps in the fossil record and uncertainties surrounding the age of key fossils have meant that these questions remain poorly understood. Here we describe and compare a highly unusual femur from Late Pleistocene sediments at Maludong (Yunnan), Southwest China, recovered along with cranial remains that exhibit a mixture of anatomically modern human and archaic traits. Our studies show that the Maludong femur has affinities to archaic hominins, especially Lower Pleistocene femora. However, the scarcity of later Middle and Late Pleistocene archaic remains in East Asia makes an assessment of systematically relevant character states difficult, warranting caution in assigning the specimen to a species at this time. The Maludong fossil probably samples an archaic population that survived until around 14,000 years ago in the biogeographically complex region of Southwest China.     

Comparaison de l'expression de certains caractères crâniens sur les hominidés chinois du Pléistocène récent et de l'Holocène (grotte supérieure de Zhoukoudian, sites de Longxian et de Yanqing)

The human remains recovered from “Grotte supérieure de Zhoukoudian” are the best-preserved Late Pleistocene human fossils in East Asia. For decades, as the representative of the Late Pleistocene human in East Asia, the Upper Cave skulls have been playing important role in the research of origins of modern Mongoloids and American Indians. With the advance of the origin and evolution of modern humans, more attention has been paid to the details and the mechanisms for the late Pleistocene human evolution and the formation of modern human populations. Both the origin and diversification of modern humans have been stressed. Some studies further trigger the debaters on the Upper Cave Man concerning its evolutionary level and its role in the formation of modern human populations in East Asia. To further explore these problems, we examined and compared 12 non-metric features on the 3 Late Pleistocene Upper Cave skulls and 162 Holocene individuals earthed from two archaeological sites of North China (Longxian and Yanqing). Our results indicate that 8 on the 12 features have different expression patterns between Upper Cave Man and recent Chinese leading the authors to believe that more primitive expressions appeared on the Upper Cave Man than on recent Chinese populations. Based on these findings, some problems on the intragroup variation in Late Pleistocene and Holocene populations are discussed.     

现代人的出现与扩散——中国的化石证据

自2002年在周口店附近的田园洞发现大约4万年前的现代人化石以来,相继在湖北郧西黄龙洞、广西崇左智人洞等地点发现了早期现代人化石。这些化石发现证实大约10万年前早期现代人在华南地区已经出现。最近在湖南道县福岩洞发现的人类牙齿化石及相关研究进一步揭示具有完全现代形态的人类8万-12万年前在华南局部地区已经出现;而在这个时间段的华北地区,以许家窑人为代表的人类化石形态仍较原始,其演化尚未进入早期现代人阶段。这些研究发现提示,在中国地区,华南是现代人形成与扩散的中心区域,早期现代人以及完全现代类型的人类都可能首先在华南地区出现,然后向华北地区扩散。现有的化石形态证据显示,更新世晚期华南地区人类具有较大的演化变异,可能同时生存有几种不同的演化类群。智人洞属于从古老型智人向现代人演化的过渡类型,而道县则代表着演化进入完全现代类型的人类。基于前人研究及本文的分析,作者认为柳江、资阳、丽江、田园洞等更新世晚期人类化石特征比较进步,在演化上属于与道县相似的现代类型人类。值得注意的是,这些研究进展在引起对现代人在东亚地区出现和扩散关注的同时,古人类学界对其中涉及的许多问题还存在争论。本文在回顾分析这些研究进展的基础上,就相关问题进行了讨论。     

Lower limb bone structure of Middle Pleistocene hominins from the Caune de l’Arago (Tautavel,France): Evolutionary and functional comparison with the penecontemporaneous hominins of Sima de los Huesos (Atapuerca,Spain)

The Caune de l’Arago (Arago) and Sima de los Huesos (Sima) human bones from the European Middle Pleistocene are penecontemporaneous, although the Sima hominins are closely related to Neandertal, and Arago hominins present more archaic features. In previous and in press studies, the cross-sectional geometric properties (CSG) of lower limb bones of Arago and Sima have been studied separately without comparative analyses. Here, in order to bridge this gap, we use the same criteria for both samples to highlight evolutionary affinities and to compare their level and pattern of mobility. This study focuses on the femur, fibula and tibia from Arago and Sima with references to fossils from the sites of Trinil, Zhoukoudian and Lazaret, and ancient and recent Homo sapiens (including athletes and non-athletes). We analyze the cross-sectional areas, biomechanical bone “shape” indices (Ix/Iy, Imax/Imin) and pattern of cortical bone distribution. All lower limb bones from Arago have noticeably high to very high relative cortical areas and low to very low medullary areas. The overall femoral pattern in Arago, like Sima, is similar to that of Middle Pleistocene hominins (e.g., low femoral shape indices, Ix/Iy) and Neandertals (e.g., large cross-sectional size). However, the femoral midshaft in Sima presents prominent posteromedial cortical thickening, as a result of a spiral cortical reinforcement along the medial side of the diaphysis. This characteristic is specific to Neandertal and some Middle Pleistocene hominins. In contrast, the midshaft femoral pattern in Arago is close to that of some Homo erectus. We also note that the femoral cross-sectional size and relative cortical area in Arago differ drastically to the small size and low relative cortical area of Lazaret and Trinil hominins. The very high shape index at midshaft (i.e., high Imax/Imin) of the Arago tibia is observed in ancient H. sapiens and runners; the tibial posterior “pilaster” is found in Neandertals and ancient H. sapiens; and the flat or convex tibial faces are similar to Neandertals. Furthermore, the Arago fibulas show marked fibular posterolateral cortical reinforcement with low anteroposterior strengthening. These leg features (tibia, fibula) are also found in some Sima hominins (but not in all individuals). Consequently, this study confirms the presence of archaic features in Arago and the close evolutionary relationship between Sima and Neandertal. This proposition is mainly based on the femoral midshaft pattern influenced by the pelvofemoral complex, considered to be substantially genetically controlled. The leg functional analysis highlights a high level of mobility and travelling in uneven terrains or in mountainous areas in Arago, consistent with known environments and hunting practices. Previously, an analogous hypothesis was proposed put forward for Sima hominins.     

Variation in cortical bone histology within the human femur and its impact on estimating age at death

Histological methods for the estimation of age at death using cortical bone are based on the evaluation of microstructural changes over time. Since histological analysis is a destructive method, most techniques attempt to limit the amount of cortical bone needed for analysis. Sample location, however, can have a significant effect on the accuracy of these methods. Furthermore, research demonstrates that both intersection and intrasection variation is present at the midshaft of the femur, which is the primary location for estimating age at death in humans. This research determines the extent of regional variation within the adult human femur and its effect on age estimation. Secondary osteon lamellae and Haversian canal ratio and cortical thickness were quantified. Thompson's All Males Left Femur regression equation was used to estimate age. Results show that significant regional variation occurs in the estimated ages derived from the posterior aspect of the femoral shaft and significant intrasection variation occurs in age estimates from the mid and mid-distal cross-sections. Thus, the inter and intrasection variation that occurs in bone remodeling within the femoral cortex has the potential to produce significant differences amongst age estimates taken from various femoral diaphyseal locations compared to the age estimated from the standard location used in Thompson's core method (1978). The results indicate that the use of this histological method is dependant on the ability to correctly identify the four anatomical locations, but the extracted core used for age estimation is not necessarily confined to the anterior midshaft.     

Hominin teeth from the early Late Pleistocene site of Xujiayao,Northern China

It is generally accepted that from the late Middle to the early Late Pleistocene (～340–90 ka BP), Neanderthals were occupying Europe and Western Asia, whereas anatomically modern humans were present in the African continent. In contrast, the paucity of hominin fossil evidence from East Asia from this period impedes a complete evolutionary picture of the genus Homo, as well as assessment of the possible contribution of or interaction with Asian hominins in the evolution of Homo sapiens and Homo neanderthalensis. Here we present a comparative study of a hominin dental sample recovered from the Xujiayao site, in Northern China, attributed to the early Late Pleistocene (MIS 5 to 4). Our dental study reveals a mosaic of primitive and derived dental features for the Xujiayao hominins that can be summarized as follows: i) they are different from archaic and recent modern humans, ii) they present some features that are common but not exclusive to the Neanderthal lineage, and iii) they retain some primitive conformations classically found in East Asian Early and Middle Pleistocene hominins despite their young geological age. Thus, our study evinces the existence in China of a population of unclear taxonomic status with regard to other contemporary populations such as H. sapiens and H. neanderthalensis. The morphological and metric studies of the Xujiayao teeth expand the variability known for early Late Pleistocene hominin fossils and suggest the possibility that a primitive hominin lineage may have survived late into the Late Pleistocene in China. Am J Phys Anthropol 156:224–240, 2015. © 2014 Wiley Periodicals, Inc.     

Late pleistocene human femoral diaphyseal curvature

Anterior femoral curvature is a consistent characteristic of Pleistocene and recent humans, although variation exists in the degree of curvature among individuals and across populations. In particular, one group, the Neandertals, has been characterized for a century as having marked femoral curvature. To evaluate the degree of anterior femoral curvature in both Neandertals and other Late Pleistocene humans, their curvature subtenses and proximodistal positions were evaluated in the context of recent human variation. Recent human comparisons show little relationship between subtense (absolute curvature) and femoral length, suggesting that an index that incorporates subtense relative to the length of the femur is inappropriate for between-group assessments. Neandertals were statistically indistinguishable from Middle or earlier Upper Paleolithic modern humans in the degree of absolute curvature, all of whom had greater curvature on average than all later humans. Additionally, Neandertals and Qafzeh-Skhul early modern humans had a more distal point of maximum curvature than any other group. Curvature was not strongly correlated with functional considerations including body mass estimates, surrogate variables for body size, proximal femoral articular orientation, or knee anteroposterior dimensions. The functional role of femoral anterior curvature is unknown; however, the general decrease in curvature subtense closely parallels the between-group changes in inferred levels of mobility from femoral diaphyseal robusticity and shape, suggesting that femoral curvature may reflect mobility levels and patterns among Late Pleistocene and recent humans.